Longitudinal structure of the vertical E × B drift and ion density seen from ROCSAT‐1

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Tropospheric tidal effects on the middle and upper atmosphere (2009, background): “[2] Recent satellite borne diagnostics of the low-latitude upper atmosphere reveal longitude variations in 1356 nm airglow brightness measurements [e.g., Sagawa et al., 2005; Immel et al., 2006; England et al., 2006b], electron density [Lin et al., 2007; Lu¨hr et al., 2007], electric field [England ”
Electrodynamics of the formation of ionospheric wave number 4 longitudinal structure (2008, methodology): “During the daytime, wave number 4 structure has been observed both in the ionospheric density and the vertical E � B drift [Lin et al., 2007b; Kil et al., 2007 ]; thus, the longitudinal variation of E � B drift is probably the primary driver for that of the ionospheric density, whereas in the eveni”
Wavenumber‐4 patterns of the total electron content over the low latitude ionosphere (2008, background): “…the longitudinal wavenumber-4 structure also occurred in other parameters such as the vertical ion drift velocity, the electron temperature, and even in the zonal neutral wind in the F region [Hartman and Heelis, 2007; Ren et al., 2008; Kil et al., 2007; Häusler et al., 2007; Lühr et al., 2007].”